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Torbjorn M.J. Nilsson

Researcher at Chalmers University of Technology

Publications -  33
Citations -  1136

Torbjorn M.J. Nilsson is an academic researcher from Chalmers University of Technology. The author has contributed to research in topics: Radiative cooling & Thermal resistance. The author has an hindex of 12, co-authored 31 publications receiving 923 citations. Previous affiliations of Torbjorn M.J. Nilsson include Uppsala University & Saab AB.

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Novel nanostructured thermal interface materials: a review

TL;DR: In this paper, the authors identify the key areas for state-of-the-art thermal interface materials (TIMs) research and investigate the current state of the field together with possible future advances.
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Radiative cooling during the day: simulations and experiments on pigmented polyethylene cover foils

TL;DR: In this paper, a 400 μm thick ZnS pigmented polyethylene foil with a pigment volume fraction of 0.15 and a solar reflectance of 1.849 was tested in Tanzania.
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Dew water collector for potable water in Ajaccio (Corsica Island, France)

TL;DR: In this article, the authors report on the development of an inexpensive radiative condenser for collecting atmospheric vapor based on the experience gained using a small working model in Grenoble (France), a prototype of 10×3 m2 was established in Ajaccio (Corsica, France).
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A solar reflecting material for radiative cooling applications : ZnS pigmented polyethylene

TL;DR: In this paper, the authors compared the optical properties of ZnS pigmented polyethylene foils with various thicknesses and volume fractions of pigments, and showed that the optimum solar reflectance of the foil is 0.825 for the available pigment powder; it should be 0.88 if heating were to be avoided at noon with the sun in its zenith.
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Initial experiments on dew collection in Sweden and Tanzania

TL;DR: In this paper, observations of dew formation on radiatively cooled pigmented polyethylene foils were carried out in Sweden and in arid Dodoma, Tanzania, and the results were in agreement with thermodynamic calculations, though the variation is large in the daily measured dew water volumes.